Search results for "Cristobalite"

showing 10 items of 16 documents

Batch-to-Melt Conversion Kinetics in Sodium Aluminosilicate Batches Using Different Alumina Raw Materials

2016

The batch-to-melt conversion in batches of sand, soda ash and corundum (C), alumina spinel (A), boehmite (B), or gibbsite (G) as Al2O3 carrier are studied using thermal analysis, X-ray diffraction, and 27Al nuclear magnetic resonance spectroscopy. Laboratory-scaled batches are either heated continuously or quenched from 1600°C in a series of increasing dwell times. The results show that the conversion from the raw materials to the fresh melt proceeds in two kinetic stages. During the first stage (3–5 min), fast conversion of nearly 95% by mass occurs and the conversion coefficient increases in the order G < C ≈ A < B. The second stage is controlled by the slow dissolution of intermediate cr…

010302 applied physicsBoehmiteMaterials scienceSpinelAnalytical chemistryMineralogyCorundum02 engineering and technologyengineering.material021001 nanoscience & nanotechnology01 natural sciencesCristobalitechemistry.chemical_compoundchemistry0103 physical sciencesengineeringGeneral Materials Science0210 nano-technologyThermal analysisDissolutionGibbsiteSodium aluminosilicateInternational Journal of Applied Glass Science
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Luminescence of polymorphous SiO2

2016

Abstract The luminescence of self-trapped exciton (STE) was found and systematically studied in tetrahedron structured silica crystals (α-quartz, coesite, cristobalite) and glass. In octahedron structured stishovite only host material defect luminescence was observed. It strongly resembles luminescence of oxygen deficient silica glass and γ or neutron irradiated α-quartz. The energetic yield of STE luminescence for α-quartz and coesite is about 20% of absorbed energy and about 5(7)% for cristobalite. Two types of STE were found in α-quartz. Two overlapping bands of STEs are located at 2.5–2.7 eV. The model of STE is proposed as Si–O bond rupture, relaxation of created non-bridging oxygen (N…

010302 applied physicsRadiationMaterials scienceMineralogy02 engineering and technologyElectronic structureengineering.material021001 nanoscience & nanotechnology01 natural sciencesCristobalitesymbols.namesakeCrystallographyOctahedron0103 physical sciencesCoesitesymbolsengineering0210 nano-technologyRaman spectroscopyLuminescenceInstrumentationStishoviteNatural bond orbitalRadiation Measurements
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Effect of Alkali Ions on the Amorphous to Crystalline Phase Transition of Silica

2001

Abstract The effect of the addition of alkali ions to commercial amorphous silica, generally used as support for heterogeneous catalysts, has been investigated from the point of view of morphological and structural changes. Samples of alkali-doped silica were prepared by impregnation and subsequent calcination at various temperatures. The structural effect of Li, Na, K, and Cs was determined by use of techniques such as wide-angle (WAXS) and small-angle X-ray scattering (SAXS). The WAXS diffractograms, analyzed with the Rietveld method using the GSAS program, allowed qualitative and quantitative identification of the fraction of the different silica polymorphs like quartz, tridymite, and cr…

ChemistrySmall-angle X-ray scatteringInorganic chemistryAnalytical chemistryCrystal structureCondensed Matter PhysicsCristobaliteElectronic Optical and Magnetic Materialslaw.inventionAmorphous solidInorganic ChemistrySurface areaTridymitelawMaterials ChemistryCeramics and CompositesCalcinationPhysical and Theoretical ChemistryCrystallizationJournal of Solid State Chemistry
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The formation of silica high temperature polymorphs from quartz: Influence of grain size and mineralising agents

2015

Abstract The formation of high-temperature silica polymorphs in presence of Na and K has been studied at various temperatures and soaking times, starting from quartzes of different grain size, ex situ as well as in situ. The results show that cristobalite and tridymite formation is strongly influenced by the nature and the amount of mineraliser added. In particular, K seems to discriminate more between the two structures, as it produces the largest observed amount of cristobalite. The disappearance of quartz can be controlled by the proper combination of mineraliser/temperature/time, which in turn control the amount and the type of polymorph formed, together with the amount of amorphous mat…

Materials Chemistry2506 Metals and AlloysPhase transitionMaterials scienceMineraliser; Phase transition; Silica polymorphs; Ceramics and Composites; Materials Chemistry2506 Metals and AlloysCeramics and CompositeCristobaliteGrain sizeAmorphous solidSilica polymorphMineraliser; Phase transition; Silica polymorphsCrystallographyTridymiteChemical engineeringLinear combination of atomic orbitalsvisual_artMineraliserMaterials ChemistryCeramics and Compositesvisual_art.visual_art_mediumCeramicQuartzSilica polymorphsPhase transition
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Effects of Pressure, Thermal Treatment, and O2 Loading in MCM41, MSU-H, and MSU-F Mesoporous Silica Systems Probed by Raman Spectroscopy

2015

We present a Raman study of the effects induced by pressure, thermal treatments, and O2 loading in MCM41, MSU-H, and MSU-F representative mesoporous silica. We compared the starting powders with the mechanically pressed tablets produced applying pressures of ∼0.2 and ∼0.45 GPa. The spectra of the three untreated tablets evidence that the main value of the Si-O-Si angle decreases and that in the MCM41 and the MSU-H Si-O-Si hydrolysis occurs, whereas such a process is absent or much less efficient in the MSU-F. Despite their different networks, the three powders tend to crystallize in cristobalite when treatments are at 1000 °C. The MCM41 and MSU-H tablets exhibit behavior similar to their st…

Materials scienceElectronic Optical and Magnetic MaterialSettore FIS/01 - Fisica SperimentaleMineralogySurfaces Coatings and FilmThermal treatmentMesoporous silicaCristobaliteSurfaces Coatings and FilmsElectronic Optical and Magnetic Materialssymbols.namesakeHydrolysisGeneral EnergyTridymiteEnergy (all)Chemical engineeringPhase (matter)symbolsMoleculePhysical and Theoretical ChemistryRaman spectroscopy
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Thermal decomposition of chromite spinel with chlorite admixture

2008

Abstract The behaviour of minerals in a South African chromite ore during the increasing of the temperature has been studied. Firstly, the changes produced during the ignition process have been examined by means of thermal and differential analysis (TGA–DTA) until 1200 °C. The characterization of the initial mineral and those obtained after heating at several temperatures in room atmosphere has been performed by X-ray diffraction (XRD). Moreover, voltammetric analyses have allowed to determine the variation of the iron oxidation degree in the studied materials. Light microscopy was applied to find more information about the different phases by their colour. During the heating, a wide range …

MetallurgySpinelThermal decompositionOxideengineering.materialCondensed Matter PhysicsCristobalitechemistry.chemical_compoundchemistryChemical engineeringDifferential thermal analysisengineeringChromitePhysical and Theoretical ChemistryThermal analysisInstrumentationMagnetiteThermochimica Acta
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Aluminum-27 double-rotation NMR investigations of SAPO-5 with variable silicon content

1995

Summary Double-rotation NMR (DOR) studies of 27 Al species in SAPO-5, a silicon aluminophosphate molecular sieve with a one dimensional channel system, have revealed a minimum of three aluminum sites resulting from the synthesis. The DOR technique was used specifically to increase the spectral resolution by removing the broadening influences from second-order quadrupolar interactions associated with the spin 5/2 27 Al nuclei. The DOR investigations of SAPO-5 crystals with variable Si/Al ratios resulted in the identification of three aluminum species, two consistent with the reported isotropic shift values for AlPO 4 -5; however, these two resonances are only observable when small quantities…

NMR spectra databaseNuclear magnetic resonanceSiliconchemistryAluminiumPhase (matter)Analytical chemistrychemistry.chemical_elementResonanceSpin (physics)Molecular sieveCristobalite
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Evidence for fractional condensation and reprocessing at high temperatures in CH chondrites

2003

We performed a detailed study of silica-rich components (SRC) in the paired CH chondrites Acfer 182 and 207. These SRCs appear either as chondrules or fragments, and they contribute <0.1 vol% to the bulk meteorite. They usually contain a silica and a silicate portion. Both portions are, in most cases, cryptocrystalline and have bulk SiO2-concentrations between 65 and 85 wt%. The silicate generally has a pyroxene normative composition. The silica often appears as blebs within the silicate matrix or vice versa. If there are no blebs, silica and silicate still form rounded interfaces. The SRCs are depleted in refractory elements like Ca, Al, and Ti relative to CI. A few SRC- like objects are e…

OlivineAnalytical chemistryChondruleMineralogyPyroxeneForsteriteengineering.materialCristobaliteSilicatechemistry.chemical_compoundGeophysicschemistrySpace and Planetary ScienceChondriteEnstatiteengineeringGeologyMeteoritics &amp; Planetary Science
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Synthesis and reactivity of cristobalite obtained from the SiO2-V2O5 system

1990

On etudie par diffraction RX l'evolution des phases cristallines lors de la cuisson a 650-1250 o C de compositions du systeme ZrO 2 −V 2 O 5 −SiO 2 et la reactivite de la cristobalite preparee avec la phase ZrO 2 monoclinique

Oxide ceramicsMaterials scienceInorganic chemistryX-ray crystallographyPhysical chemistryGeneral Materials ScienceReactivity (chemistry)CristobaliteJournal of Materials Science Letters
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The genesis of actively growing siliceous stromatolites: Evidence from Lake Specchio di Venere, Pantelleria Island, Italy

2010

This study documents the attributes of siliceous stromatolites growing in the Lake Specchio di Venere, on the volcanic island of Pantelleria, Italy, in a setting characterized by very shallow cold waters and pools and by scattered hydrothermal activity, which exhales mainly CO2, at emission point temperatures of 34 to 58 °C. The saturation indexes indicate that the lake waters are saturated with respect to tridymite, cristobalite, chalcedony and quartz, and slightly undersaturated with respect to amorphous silica. Common roughly laminated and poorly lithified stromatolites show scanning electron microscope (SEM) evidence for silicified microbial mat structures, including biofilms, filamento…

Silica mineralizationMicrobial communitieSaline lakeChalcedonyMineralogyengineering.materialSettore BIO/19 - Microbiologia GeneraleStromatoliteTridymiteHydrothermal activityGeochemistry and PetrologyMicrobial matLithificationQuartzbiologyEarly diagenesiSettore GEO/07 - Petrologia E PetrografiaGeologybiology.organism_classificationCristobaliteSettore GEO/08 - Geochimica E VulcanologiaDiagenesisStromatoliteDNA contentengineeringGeologyChemical Geology
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